Ikari, Matt J; Fagereng, Åke (2020): Frictional velocity dependence of laboratory shearing experiments [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.914426, In: Ikari, MJ; Fagereng, Å (2020): Laboratory friction measurements of high-grade minerals [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.914429
Always quote citation above when using data! You can download the citation in several formats below.
Published: 2020-04-06 • DOI registered: 2020-05-14
Related to:
Fagereng, Åke; Ikari, Matt J (2020): Low-Temperature Frictional Characteristics of Chlorite-Epidote-Amphibole Assemblages: Implications for Strength and Seismic Style of Retrograde Fault Zones. Journal of Geophysical Research: Solid Earth, 125(4), e2020JB019487, https://doi.org/10.1029/2020JB019487
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Experiment | Exp | Ikari, Matt J | |||
| 2 | Sample comment | Sample comment | Ikari, Matt J | |||
| 3 | Sliding velocity | V | µm/s | Ikari, Matt J | Vo | |
| 4 | Sliding velocity | V | µm/s | Ikari, Matt J | V | |
| 5 | Constant | Const | Ikari, Matt J | a | ||
| 6 | Constant | Const | Ikari, Matt J | b1 | ||
| 7 | Critical slip distance | Dc | µm | Ikari, Matt J | Dc1 | |
| 8 | Constant | Const | Ikari, Matt J | b2 | ||
| 9 | Critical slip distance | Dc | µm | Ikari, Matt J | Dc2 | |
| 10 | Parameter | Parameter | arbitrary units | Ikari, Matt J | a-b | |
| 11 | Standard deviation | Std dev | ± | Ikari, Matt J | std a | |
| 12 | Standard deviation | Std dev | ± | Ikari, Matt J | std b1 | |
| 13 | Standard deviation | Std dev | ± | Ikari, Matt J | std Dc1 | |
| 14 | Standard deviation | Std dev | ± | Ikari, Matt J | std b2 (µm) | |
| 15 | Standard deviation | Std dev | ± | Ikari, Matt J | std Dc2 (µm) |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
947 data points
Data
| 1 Exp | 2 Sample comment | 3 V [µm/s] (Vo) | 4 V [µm/s] (V) | 5 Const (a) | 6 Const (b1) | 7 Dc [µm] (Dc1) | 8 Const (b2) | 9 Dc [µm] (Dc2) | 10 Parameter [arbitrary units] (a-b) | 11 Std dev [±] (std a) | 12 Std dev [±] (std b1) | 13 Std dev [±] (std Dc1) | 14 Std dev [±] (std b2 (µm)) | 15 Std dev [±] (std Dc2 (µm)) |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| B808 | epidotite | 0.1 | 0.3 | 0.0057 | 0.0068 | 26.9 | -0.0011 | 0.00017 | 0.00016 | 0.95 | ||||
| B808 | epidotite | 0.3 | 1.0 | 0.0052 | 0.0096 | 32.9 | 0.0026 | 119.1 | -0.0069 | 0.00007 | 0.00028 | 0.93 | 0.00028 | 11.58 |
| B808 | epidotite | 1.0 | 3.0 | 0.0045 | 0.0081 | 34.1 | -0.0037 | 0.00005 | 0.00005 | 0.33 | ||||
| B808 | epidotite | 3.0 | 10.0 | 0.0045 | 0.0067 | 19.8 | -0.0021 | 0.00018 | 0.00018 | 0.72 | ||||
| B808 | epidotite | 10.0 | 30.0 | 0.0042 | 0.0099 | 22.7 | -0.0056 | 0.00009 | 0.00009 | 0.31 | ||||
| B686 | 70% ep, 30% ch | 0.1 | 0.3 | 0.0035 | 0.0039 | 10.0 | -0.0004 | 0.00014 | 0.00014 | 0.50 | ||||
| B686 | 70% ep, 30% ch | 0.3 | 1.0 | 0.0042 | 0.0049 | 20.1 | -0.0007 | 0.00018 | 0.00018 | 0.94 | ||||
| B686 | 70% ep, 30% ch | 1.0 | 3.0 | 0.0044 | 0.0023 | 10.0 | 0.0045 | 96.8 | -0.0023 | 0.00043 | 0.00042 | 3.87 | 0.00023 | 5.62 |
| B686 | 70% ep, 30% ch | 3.0 | 10.0 | 0.0042 | 0.0033 | 17.7 | 0.0026 | 36.7 | -0.0017 | 0.00024 | 0.00013 | 2.73 | 0.00012 | 3.65 |
| B686 | 70% ep, 30% ch | 10.0 | 30.0 | 0.0038 | 0.0021 | 14.3 | 0.0040 | 127.2 | -0.0023 | 0.00071 | 0.00071 | 10.02 | 0.00039 | 14.70 |
| B813 | 70% ep, 30% ch | 0.1 | 0.3 | 0.0039 | 0.0040 | 10.1 | 0.0021 | 84.7 | -0.0023 | 0.00012 | 0.00014 | 0.60 | 0.00008 | 7.71 |
| B813 | 70% ep, 30% ch | 0.3 | 1.0 | 0.0040 | 0.0048 | 11.8 | 0.0032 | 171.7 | -0.0040 | 0.00011 | 0.00012 | 0.51 | 0.00018 | 25.26 |
| B813 | 70% ep, 30% ch | 1.0 | 3.0 | 0.0039 | 0.0039 | 7.4 | 0.0064 | 110.0 | -0.0065 | 0.00021 | 0.00021 | 0.73 | 0.00008 | 2.09 |
| B813 | 70% ep, 30% ch | 3.0 | 10.0 | 0.0042 | 0.0051 | 12.9 | 0.0054 | 115.2 | -0.0063 | 0.00011 | 0.00011 | 0.45 | 0.00005 | 2.54 |
| B813 | 70% ep, 30% ch | 10.0 | 30.0 | 0.0043 | 0.0032 | 16.8 | 0.0046 | 51.6 | -0.0034 | 0.00022 | 0.00080 | 4.62 | 0.00086 | 5.41 |
| B687 | 50% ep, 50% ch | 0.1 | 0.3 | 0.0029 | 0.0035 | 7.5 | 0.0030 | 166.3 | -0.0036 | 0.00020 | 0.00020 | 0.77 | 0.00006 | 7.41 |
| B687 | 50% ep, 50% ch | 0.3 | 1.0 | 0.0033 | 0.0032 | 8.7 | 0.0063 | 83.3 | -0.0062 | 0.00052 | 0.00052 | 2.52 | 0.00026 | 3.78 |
| B687 | 50% ep, 50% ch | 1.0 | 3.0 | 0.0038 | 0.0062 | 18.3 | -0.0024 | 0.00012 | 0.00012 | 0.45 | ||||
| B687 | 50% ep, 50% ch | 3.0 | 10.0 | 0.0033 | 0.0105 | 27.7 | -0.0078 | 48.8 | 0.0006 | 0.00012 | 0.00006 | 0.73 | 0.00006 | 1.05 |
| B687 | 50% ep, 50% ch | 10.0 | 30.0 | 0.0039 | 0.0026 | 5.3 | 0.0039 | 164.6 | -0.0025 | 0.00120 | 0.00117 | 3.84 | 0.00014 | 9.99 |
| B811 | 50% ep, 50% ch | 0.1 | 0.3 | 0.0029 | 0.0023 | 6.7 | 0.0032 | 42.5 | -0.0026 | 0.00012 | 0.00015 | 0.80 | 0.00013 | 1.62 |
| B811 | 50% ep, 50% ch | 0.3 | 1.0 | 0.0035 | 0.0031 | 9.3 | 0.0004 | 0.00011 | 0.00011 | 0.48 | ||||
| B811 | 50% ep, 50% ch | 1.0 | 3.0 | 0.0039 | 0.0018 | 13.7 | 0.0029 | 45.9 | -0.0008 | 0.00015 | 0.00035 | 3.64 | 0.00038 | 3.56 |
| B811 | 50% ep, 50% ch | 3.0 | 10.0 | 0.0037 | 0.0030 | 19.7 | 0.0007 | 0.00005 | 0.00005 | 0.48 | ||||
| B811 | 50% ep, 50% ch | 10.0 | 30.0 | 0.0041 | 0.0028 | 16.9 | 0.0036 | 122.7 | -0.0023 | 0.00008 | 0.00008 | 0.90 | 0.00006 | 2.44 |
| B692 | 30% ep, 70% ch | 0.1 | 0.3 | 0.0025 | 0.0032 | 14.4 | -0.0007 | 0.00015 | 0.00015 | 0.90 | ||||
| B692 | 30% ep, 70% ch | 0.3 | 1.0 | 0.0022 | 0.0007 | 7.9 | 0.0025 | 82.8 | -0.0011 | 0.00012 | 0.00012 | 2.78 | 0.00007 | 2.68 |
| B692 | 30% ep, 70% ch | 1.0 | 3.0 | 0.0027 | 0.0020 | 76.1 | 0.0007 | 0.00005 | 0.00004 | 2.87 | ||||
| B692 | 30% ep, 70% ch | 3.0 | 10.0 | 0.0042 | 0.0022 | 135.2 | 0.0019 | 0.00005 | 0.00005 | 5.07 | ||||
| B692 | 30% ep, 70% ch | 10.0 | 30.0 | 0.0057 | 0.0021 | 273.2 | 0.0036 | 0.00007 | 0.00007 | 20.38 | ||||
| B807 | chlorite schist | 0.1 | 0.3 | 0.0025 | 0.0016 | 40.0 | 0.0009 | 0.00004 | 0.00004 | 1.34 | ||||
| B807 | chlorite schist | 0.3 | 1.0 | 0.0030 | 0.0015 | 75.8 | 0.0015 | 0.00004 | 0.00004 | 3.12 | ||||
| B807 | chlorite schist | 1.0 | 3.0 | 0.0041 | -0.0013 | 48.7 | 0.0054 | 0.00003 | 0.00003 | 1.49 | ||||
| B807 | chlorite schist | 3.0 | 10.0 | 0.0055 | 0.0006 | 278.0 | 0.0049 | 0.00003 | 0.00009 | 102.78 | ||||
| B807 | chlorite schist | 10.0 | 30.0 | 0.0070 | -0.0068 | 97.5 | 0.0137 | 0.00013 | 0.00013 | 3.41 | ||||
| B810 | chlorite schist | 0.1 | 0.3 | 0.0032 | 0.0007 | 68.6 | 0.0025 | 0.00004 | 0.00004 | 6.72 | ||||
| B810 | chlorite schist | 0.3 | 1.0 | 0.0034 | 0.0008 | 174.2 | 0.0027 | 0.00003 | 0.00012 | 54.89 | ||||
| B810 | chlorite schist | 1.0 | 3.0 | 0.0040 | 0.0008 | 78.5 | 0.0032 | 0.00002 | 0.00012 | 20.86 | ||||
| B810 | chlorite schist | 3.0 | 10.0 | 0.0053 | 0.0016 | 148.3 | 0.0037 | 0.00002 | 0.00002 | 4.56 | ||||
| B810 | chlorite schist | 10.0 | 30.0 | 0.0070 | -0.0006 | 162.1 | 0.0076 | 0.00013 | 0.00029 | 300.26 | ||||
| B819 | 30% am, 70% ch | 0.1 | 0.3 | 0.0037 | 0.0029 | 5.5 | 0.0007 | 0.00030 | 0.00030 | 0.66 | ||||
| B819 | 30% am, 70% ch | 0.3 | 1.0 | 0.0035 | 0.0013 | 3.0 | 0.0016 | 36.4 | 0.0006 | 0.00011 | 0.00010 | 0.41 | 0.00004 | 1.20 |
| B819 | 30% am, 70% ch | 1.0 | 3.0 | 0.0032 | 0.0011 | 45.3 | 0.0021 | 0.00002 | 0.00002 | 1.51 | ||||
| B819 | 30% am, 70% ch | 3.0 | 10.0 | 0.0043 | 0.0019 | 44.1 | 0.0024 | 0.00003 | 0.00003 | 1.19 | ||||
| B819 | 30% am, 70% ch | 10.0 | 30.0 | 0.0043 | -0.0008 | 47.1 | 0.0051 | 0.00003 | 0.00002 | 2.44 | ||||
| B818 | 50% am, 50% ch | 0.1 | 0.3 | 0.0034 | 0.0031 | 12.9 | 0.0003 | 0.00029 | 0.00029 | 1.66 | ||||
| B818 | 50% am, 50% ch | 0.3 | 1.0 | 0.0031 | 0.0031 | 40.6 | 0.0000 | 0.00003 | 0.00002 | 0.83 | ||||
| B818 | 50% am, 50% ch | 1.0 | 3.0 | 0.0036 | 0.0038 | 75.8 | -0.0002 | 0.00002 | 0.00002 | 1.20 | ||||
| B818 | 50% am, 50% ch | 3.0 | 10.0 | 0.0040 | 0.0037 | 64.8 | 0.0003 | 0.00003 | 0.00003 | 0.87 | ||||
| B818 | 50% am, 50% ch | 10.0 | 30.0 | 0.0046 | 0.0013 | 61.6 | 0.0033 | 0.00004 | 0.00004 | 3.26 | ||||
| B814 | 70% am, 30% ch | 0.1 | 0.3 | 0.0036 | 0.0041 | 17.6 | -0.0005 | 0.00020 | 0.00020 | 1.22 | ||||
| B814 | 70% am, 30% ch | 0.3 | 1.0 | 0.0028 | 0.0054 | 62.6 | -0.0027 | 0.00006 | 0.00005 | 0.97 | ||||
| B814 | 70% am, 30% ch | 1.0 | 3.0 | 0.0045 | 0.0023 | 5.9 | 0.0053 | 121.4 | -0.0031 | 0.00030 | 0.00029 | 1.39 | 0.00010 | 3.53 |
| B814 | 70% am, 30% ch | 3.0 | 10.0 | 0.0037 | 0.0024 | 13.3 | 0.0014 | 0.00009 | 0.00009 | 0.73 | ||||
| B814 | 70% am, 30% ch | 10.0 | 30.0 | 0.0039 | 0.0042 | 19.2 | -0.0002 | 0.00009 | 0.00009 | 0.53 | ||||
| B809 | amphibolite | 0.1 | 0.3 | 0.0081 | 0.0234 | 284.5 | -0.0153 | 0.00007 | 0.00012 | 3.58 | 0.00009 | 2.69 | ||
| B809 | amphibolite | 0.3 | 1.0 | 0.0067 | 0.0181 | 232.6 | -0.0114 | 0.00004 | 0.00004 | 1.37 | ||||
| B809 | amphibolite | 1.0 | 3.0 | 0.0062 | 0.0022 | 34.3 | 0.0041 | 0.00013 | 0.00012 | 2.79 | ||||
| B809 | amphibolite | 3.0 | 10.0 | 0.0053 | 0.0086 | 183.7 | -0.0033 | 0.00003 | 0.00006 | 2.89 | ||||
| B809 | amphibolite | 10.0 | 30.0 | 0.0047 | 0.0065 | 72.1 | -0.0018 | 0.00005 | 0.00004 | 0.86 | ||||
| B812 | 50% ep, 50% am | 0.1 | 0.3 | 0.0066 | 0.0102 | 101.1 | -0.0036 | 0.00006 | 0.00006 | 1.16 | ||||
| B812 | 50% ep, 50% am | 0.3 | 1.0 | 0.0055 | 0.0058 | 98.6 | -0.0003 | 0.00003 | 0.00004 | 1.91 | ||||
| B812 | 50% ep, 50% am | 1.0 | 3.0 | 0.0049 | 0.0014 | 8.3 | 0.0052 | 167.0 | -0.0017 | 0.00015 | 0.00015 | 1.38 | 0.00004 | 2.42 |
| B812 | 50% ep, 50% am | 3.0 | 10.0 | 0.0045 | 0.0038 | 30.7 | 0.0056 | 162.3 | -0.0049 | 0.00010 | 0.00015 | 1.91 | 0.00014 | 3.94 |
| B812 | 50% ep, 50% am | 10.0 | 30.0 | 0.0042 | 0.0020 | 19.5 | 0.0109 | 168.1 | -0.0087 | 0.00013 | 0.00013 | 2.19 | 0.00008 | 1.47 |
| B816 | 33% ep, 33% am, 33% ch | 0.1 | 0.3 | 0.0037 | 0.0041 | 10.9 | -0.0003 | 0.00013 | 0.00013 | 0.52 | ||||
| B816 | 33% ep, 33% am, 33% ch | 0.3 | 1.0 | 0.0037 | 0.0011 | 4.7 | 0.0074 | 49.1 | -0.0048 | 0.00019 | 0.00019 | 2.06 | 0.00012 | 0.89 |
| B816 | 33% ep, 33% am, 33% ch | 1.0 | 3.0 | 0.0043 | 0.0017 | 6.0 | 0.0062 | 68.3 | -0.0036 | 0.00019 | 0.00019 | 1.12 | 0.00008 | 1.03 |
| B816 | 33% ep, 33% am, 33% ch | 3.0 | 10.0 | 0.0045 | 0.0020 | 10.3 | 0.0045 | 46.9 | -0.0019 | 0.00029 | 0.00046 | 4.12 | 0.00046 | 3.55 |
| B816 | 33% ep, 33% am, 33% ch | 10.0 | 30.0 | 0.0045 | 0.0043 | 19.3 | 0.0009 | 112.2 | -0.0007 | 0.00010 | 0.00015 | 1.07 | 0.00012 | 32.51 |
| B694 | 33% ep, 33% am, 33% ch | 0.1 | 0.3 | 0.0039 | 0.0022 | 9.3 | 0.0065 | 117.9 | -0.0048 | 0.00026 | 0.00026 | 1.84 | 0.00010 | 2.94 |
| B694 | 33% ep, 33% am, 33% ch | 0.3 | 1.0 | 0.0036 | 0.0022 | 10.8 | 0.0031 | 220.2 | -0.0017 | 0.00012 | 0.00012 | 0.93 | 0.00006 | 11.74 |
| B694 | 33% ep, 33% am, 33% ch | 1.0 | 3.0 | 0.0043 | 0.0027 | 8.7 | 0.0016 | 0.00021 | 0.00021 | 0.98 | ||||
| B694 | 33% ep, 33% am, 33% ch | 3.0 | 10.0 | 0.0046 | 0.0024 | 6.3 | 0.0024 | 68.5 | -0.0002 | 0.00039 | 0.00038 | 1.84 | 0.00017 | 6.23 |
| B694 | 33% ep, 33% am, 33% ch | 10.0 | 30.0 | 0.0048 | 0.0026 | 8.3 | 0.0015 | 226.3 | 0.0008 | 0.00046 | 0.00045 | 2.19 | 0.00009 | 42.28 |
